• Publications
  • Influence
Two pulses of extinction during the Permian–Triassic crisis
Over 90% of marine species were lost during the end-Permian extinction. Fossil data show that the crisis in China was marked by two distinct phases of marine extinction separated by a 180,000-yearExpand
  • 221
  • 11
  • PDF
Abstract The fossils described here were collected from the Lower Triassic (Olenekian) at two Majiashan sections in Chaohu City, Anhui Province, East China. Nine species belonging to five genera areExpand
  • 37
  • 11
End-Permian Mass Extinction of Foraminifers in the Nanpanjiang Basin, South China
Abstract Newly obtained foraminifer faunas from the Permian-Triassic (P-Tr) transition at the Dajiang and Bianyang sections in the Nanpanjiang Basin, South China, comprise 61 species in 40 genera.Expand
  • 64
  • 9
Trace fossil evidence for restoration of marine ecosystems following the end-Permian mass extinction in the Lower Yangtze region, South China
Abstract Unlike the high-abundance, low-diversity macrofaunas that characterize many Early Triassic benthic palaeocommunities, ichnofossils were relatively common in the aftermath of the end-PermianExpand
  • 86
  • 8
Isotopic evidence for an anomalously low oceanic sulfate concentration following end-Permian mass extinction
Abstract The cataclysmic end-Permian mass extinction was immediately followed by a global expansion of microbial ecosystems, as demonstrated by widespread microbialite sequences (disaster facies) inExpand
  • 111
  • 7
  • PDF
Evolutionary dynamics of the Permian–Triassic foraminifer size: Evidence for Lilliput effect in the end-Permian mass extinction and its aftermath
Abstract There is growing evidence of the Lilliput effect in the end-Permian mass extinction and its aftermath. However, very little has been published on assessing the Lilliput effect on protozoansExpand
  • 69
  • 7
Events during Early Triassic recovery from the end-Permian extinction
The Palaeozoic–Mesozoic transition is characterized not only by the biggest Phanerozoic mass extinction, at the end of Permian, but also a prolonged period of recovery of the biota during theExpand
  • 64
  • 7
Anoxia/high temperature double whammy during the Permian-Triassic marine crisis and its aftermath
The Permian-Triassic mass extinction was the most severe biotic crisis in the past 500 million years. Many hypotheses have been proposed to explain the crisis, but few account for the spectrum ofExpand
  • 127
  • 6
  • PDF
The protracted Permo-Triassic crisis and multi-episode extinction around the Permian–Triassic boundary
Abstract The Permo-Triassic crisis was a major turning point in geological history. Following the end-Guadalupian extinction phase, the Palaeozoic biota underwent a steady decline through theExpand
  • 171
  • 6
Composition and structure of microbialite ecosystems following the end-Permian mass extinction in South China
After the end-Permian mass extinction, microbialites were widespread in the shallow marine environments in South China. Diverse microbialites are characteristic of the Early Triassic carbonateExpand
  • 89
  • 6